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Detailed Reference Information |
Buick, I.S., Uken, R., Gibson, R.L. and Wallmach, T. (1998). High-delta C-13 Paleoproterozoic carbonates from the Transvaal Supergroup, South Africa. Geology 26(10): 875-878. |
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Marbles from the Transvaal Supergroup (Kaapvaal craton, South Africa) record two positive carbon isotope excursions to average delta(13)C(carbonate) values of similar to+6 parts per thousand to +8 parts per thousand (relative to V-PDB), separated by carbonates with normal-marine delta(13)C values (similar to 0 parts per thousand +/- 2 parts per thousand). These elevated values have been preserved through metamorphic devolatilization. Together with an already documented high-C-13 excursion in overlying rocks, three separate positive carbon isotope excursions occurred on the Kaapvaal craton in the interval 2.43 to 1.93 Ga. It is not yet clear how many of these excursions reflect global rather than local processes. |
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BACKGROUND DATA FILES |
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Abstract |
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Table Dr1A |
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Table Dr1B |
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Analytical Methods & Sampling |
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Stable Isotope Data |
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Keywords
isotope geochemistry, bushveld complex, rocks, sedimentary, province, oxygen, age |
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Publisher
The Geological Society of America P.O. Box 9140 Boulder, CO 80301 1-303-447-2020 1-303-357-1071 member@geosociety.org |
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